河北武安洪山正长岩杂岩体成因与地表快速隆升-剥蚀特征

张波; 张晓旭; 苏尚国; 莫宣学; 刘江涛; 伍月; 蒋校

doi:10.3799/dqkx.2020.040

Volume 45 Issue 7

Jul. 2020

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Article Navigation > Earth Science > 2020 > 45(7): 2571-2584

Zhang Bo, Zhang Xiaoxu, Su Shangguo, Mo Xuanxue, Liu Jiangtao, Wu Yue, Jiang Xiao, 2020. Genesis and Rapid Uplift-Erosion Characteristic of Hongshan Syenite Complex in Wuan, Hebei, China. Earth Science, 45(7): 2571-2584. doi: 10.3799/dqkx.2020.040

Citation:

Zhang Bo, Zhang Xiaoxu, Su Shangguo, Mo Xuanxue, Liu Jiangtao, Wu Yue, Jiang Xiao, 2020. Genesis and Rapid Uplift-Erosion Characteristic of Hongshan Syenite Complex in Wuan, Hebei, China. Earth Science, 45(7): 2571-2584. doi: 10.3799/dqkx.2020.040

Citation:

Zhang Bo, Zhang Xiaoxu, Su Shangguo, Mo Xuanxue, Liu Jiangtao, Wu Yue, Jiang Xiao, 2020. Genesis and Rapid Uplift-Erosion Characteristic of Hongshan Syenite Complex in Wuan, Hebei, China. Earth Science, 45(7): 2571-2584. doi: 10.3799/dqkx.2020.040

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Genesis and Rapid Uplift-Erosion Characteristic of Hongshan Syenite Complex in Wuan, Hebei, China

doi: 10.3799/dqkx.2020.040

1.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
2.
Development and Research Center, China Geological Survey, Beijing 100037, China
3.
Shenyang Geological Survey Center, China Geological Survey, Shenyang 110034, China
4.
China Aero Geophysical Survey & Remote-Sensing Center for Land Resources, Beijing 100083, China

Received Date: 2020-03-08
Publish Date: 2020-07-15

Abstract

Abstract

In order to understand the source and genesis of the Hongshan syenite complex, and the rapid surface uplift-erosion phenomenon accompanying its formation, on the basis of detailed field geological surveys, petrology and geochemistry, U-Pb chronology and zircon Lu-Hf isotope studies were used. The result show that:the U-Pb dating of coarse pyroxene syenite and trachyte zircon in the Hongshan syenite complex yields age of 125.6±1.2 Ma and 121.9±2.3 Ma, respectively. Coarse syenite's age is between 125.6±1.2 Ma and 121.9±2.3 Ma, The rock belongs to high-silicon, alkali-rich, aluminum-rich, magnesium-depleted, and low-Mg^# metaluminous-peraluminous alkaline rocks, that have undergone a lot of crustal fluid transformation; coarse pyroxene syenite. Coarse-grained pyroxene syenite zircon has a similar core-edge structure of common developmental age. The core ε_Hf (t) is -5.0 to -8.4, which has a high U, Th, and Pb content. The edges are consistent with the zircon characteristics of the trachyte at the same period, ε_Hf (t)=-11.3 to -14.4, and low content of U, Th, and Pb, which indicates that the magma in the early stage of crystallization of zircon has the characteristics of crustal origin. the coarse-faced rocks of the ejected facies are directly covered on the coarse-grained ortho rocks of the central facies. This phenomenon indicates that the formation process of Hongshan syenite complex was accompanied by rapid uplift and erosion of the surface. The formation process of the Hongshan syenite complex is closely related to demolition, which is the response of the North China Craton thinning in the shallow surface.
- syenite complex,
- Mesozoic,
- zircon U-Pb chronology,
- geochemistry,
- Lu-Hf isotope,
- uplift-erosion,
- craton thinning

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References(54)

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